1.4 Sea-Floor Spreading



Vocabulary:



subduction-process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle
mid-ocean ridge-longest chain of mountains in the world
sonar-device that bounces sound waves off underwater objects and then records the echoes of these sound waves
sea-floor spreading-process that continually adds new material to the ocean floor
deep-ocean trenches-deep underwater canyons

Outline:


Summary

  • There are many bizzare animals deep under the water

Mapping the Mid-Ocean Ridge

  • curves like seam of baseball
  • under hundred of meters of water
  • more than 50,000 kilometers long

Evidence from Sea-Floor Spreading

  • At the mid-ocean ridge, molten material rises from the mantle and erupts.
  • The molten material then spreads out pushing older rock to both sides of the ridge
  • Evidence from Molten Material
    • found strange rocks shaped like:
      • pillows
      • toothpaste
    • such rocks can form only when molten material hardens quickly after erupting under water
  • Evidence from Magnetic Stripes
    • when cooled, iron bits inside lined up in direction of Earth's magnetic poles
    • rocks hardened at the same time has the same magnetic memory
    • when rocks hardened completely, it locked the iron bits in place giving the rocks a permanent "magnetic memory"
  • Evidence from Drilling Samples
    • found-the farther from ridge the sample was taken, the older the rocks were-shows sea-floor spreading took place

Subduction at Deep-Ocean Trenches

  • convection currents under the lithosphere pushes new crust that forms at the mid-ocean ridge away from the ridge and toward a deep ocean trench
  • at deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle for over tens of million years

Subduction and Earth's Oceans

    • Sea-floor spreading can change the size and shape of the ocean
  • Subduction in the Pacific Ocean
    • the Pacific Ocean is shrinking because sometimes a deep-ocean trench swallows more oceanic crust than the mid-ocean ridge can make
  • Subduction in the Atlantic Ocean
    • the Atlantic Ocean is expanding because it only has a few short trenches so the ocean floor has nowhere to go